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About: Crane Glacier     Goto   Sponge   NotDistinct   Permalink

An Entity of Type : yago:YagoPermanentlyLocatedEntity, within Data Space : dbpedia.org:8891 associated with source document(s)

Type: Thingplacedbo:Locationschema:Placenatural placeglaciergeo:SpatialThingGlacieryago:GeologicalFormation109287968yago:Glacier109289331yago:IceMass109309292yago:Object100002684yago:PhysicalEntity100001930yago:WikicatGlaciersOfGrahamLandyago:YagoGeoEntityyago:YagoPermanentlyLocatedEntity New Facet based on Instances of this Class

Crane Glacier (65°20′S 62°15′W / 65.333°S 62.250°W), is a narrow glacier which flows 30 miles (50 km) in an east-northeasterly direction along the northwest side of Aristotle Mountains to enter Spillane Fjord south of Devetaki Peak, on the east coast of the Antarctic Peninsula. Sir Hubert Wilkins photographed this feature from the air in 1928 and gave it the name "Crane Channel", after of Los Angeles, reporting that it appeared to be a channel cutting in an east-west direction across the peninsula. The name was altered to "Crane Inlet" following explorations along the west coast of the peninsula in 1936 by the British Graham Land Expedition, which proved that no through channel from the east coast existed as indicated by Wilkins. Comparison of Wilkins' photograph of this feature with th